In Peru and Tibet, Thompson has pulled
long vertical columns, or cores, of ice from the hearts of glaciers.
The Action Center sticks to the far right of the screen, and doesn't expand or cater to the extra screen real - estate on an ultrawide, this is to be expected however as there's not really much an Action Center can do other than be
a long vertical column, so no complaints from me on that regard.
Not exact matches
«The closed fingers of the massive hand fill the
long rectangular plinth, while the stupendous
vertical thumb offers a 21st century answer to Nelson's
Column itself.»
For example, nearly all recent model intercomparisons show that AOGCMs poorly reproduce precipitation in 30 ° S - 30 ° N, they still diverge for cloud cover evolution at different levels of the
vertical column, and I don't clearly understand for my part how we can speculate on
long term trends of tropospheric T without a good understanding of these convection - condensation - precipitation process.
To simplify the analysis and to make comparisons easier, it is convenient to determine how
long a horizontal tube at a single temperature and pressure would need to be to hold the same amount of air that actually exists in
vertical column.
This mission is accomplished through
long - term observations and intensive field programs that measure total
column ozone, ozone
vertical profiles (ozonesondes and umkehrs), ground level ozone, and water vapor
vertical profiles in the upper troposphere and stratosphere.
However, plotting out the high and low tiers for each practice
vertical here would make this
column unbearably
long!